Enviar artigo por via de e-mail A postseismic process in the area of the Simushir 11/2006 Earthquake recovered by the GRACE data
- Autores: Mikhailov V.O.1,2, Timoshkina E.P.1, Diament M.2
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Afiliações:
- Schmidt Institute of Physics of the Earth
- Institut de Physique du Globe de Paris
- Edição: Volume 471, Nº 1 (2016)
- Páginas: 1188-1192
- Seção: Geophysics
- URL: https://journals.rcsi.science/1028-334X/article/view/189122
- DOI: https://doi.org/10.1134/S1028334X16110179
- ID: 189122
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Resumo
The GRACE data make it possible to detect the areas where the earthquakes initiate postseismic creep in regions much larger than the focal area. This information is important for estimation of the seismic potential and position of the locked segments in the subduction zones.
Sobre autores
V. Mikhailov
Schmidt Institute of Physics of the Earth; Institut de Physique du Globe de Paris
Autor responsável pela correspondência
Email: mikh@ifz.ru
Rússia, ul. Bolshaya Gruzinskaya 10, Moscow, 123995; Paris
E. Timoshkina
Schmidt Institute of Physics of the Earth
Email: mikh@ifz.ru
Rússia, ul. Bolshaya Gruzinskaya 10, Moscow, 123995
M. Diament
Institut de Physique du Globe de Paris
Email: mikh@ifz.ru
França, Paris
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